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Wavelet analysis of deep-tow magnetic profiles: Modeling the magnetic layer thickness over oceanic ridges ArchiMer
Pouliquen, G; Sailhac, P.
The interpretation of marine magnetic anomalies usually consists either in determining the magnetization distribution assuming the source geometry and magnetization direction or in determining the magnetic layer thickness assuming the magnetization direction and intensity. In this paper, we introduce a new technique that allows modeling of the thickness of the magnetic source layer with very few a priori assumptions about the magnetization: the magnetic layer is assumed to be made of a series of bodies, each having a constant unknown magnetization and an unknown size. This technique is based upon the application of the continuous wavelet transform recently introduced for the interpretation of potential field data as a multipole decomposition. We present...
Tipo: Text Palavras-chave: Wavelet transform; Multipole decomposition; Magnetic anomalies; Source layer thickness; Mid-ocean ridges.
Ano: 2003 URL: https://archimer.ifremer.fr/doc/00224/33551/32040.pdf
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